Proceedings of the International School of Physics "Enrico Fermi.", Volume 70N. Zanichelli, 1978 - Nuclear physics |
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Page 31
sublattice is random . However , for a given substitution , there is a given average
component of the moment of the Fe3 + ions in the unsubstituted sublattice
antiparallel to the Fe3 + ion moment in the substituted sublattice . We refer to this
...
sublattice is random . However , for a given substitution , there is a given average
component of the moment of the Fe3 + ions in the unsubstituted sublattice
antiparallel to the Fe3 + ion moment in the substituted sublattice . We refer to this
...
Page 91
This behaviour indicates that the theory in the present form is not appropriate to
describe the temperature variation of the anisotropy constants of a many -
sublattice system exhibiting a compensation point . In particular , the
representation of ...
This behaviour indicates that the theory in the present form is not appropriate to
describe the temperature variation of the anisotropy constants of a many -
sublattice system exhibiting a compensation point . In particular , the
representation of ...
Page 403
... to a ground state with a finite orbital angular momentum . The results of this
treatment suggest a simple apportionment of rotation among magnetic sublattices
. For a three - sublattice rare - earth iron garnet this might be written ( 18 ) Ø = ( 4.
... to a ground state with a finite orbital angular momentum . The results of this
treatment suggest a simple apportionment of rotation among magnetic sublattices
. For a three - sublattice rare - earth iron garnet this might be written ( 18 ) Ø = ( 4.
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Contents
Magnetooptical rotation | 2 |
Rareearth iron garnets | 5 |
Bubble translation | 8 |
Copyright | |
35 other sections not shown
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Common terms and phrases
absorption angle anisotropy Appl applied assumed axis Bloch lines bubble calculated causes centres composition consider constants contribution corresponding coupling crystal cubic curve dependence determined direction discussed distribution domain effects electron energy equation exchange experiment experimental expression Fe2+ Fe3+ ions ferrimagnetic field film function GELLER give given ground increases interaction iron garnets Journ lattice levels light magnetic field magnitude material measurements mode moments motion normal observed obtained occur octahedral orientation parallel parameter photoinduced Phys plane polarization position properties rare-earth ions region relation relaxation represents resonance respectively rotation sample shown in fig shows space group specimens spin wave spontaneous spontaneous magnetization structure sublattice substitution surface symmetry temperature tetrahedral theory tion torque transition uniaxial unit values variation wall yttrium iron garnet
References to this book
Structural and Magnetic Phase Transitions in Minerals S. Ghose,J.M.D. Coey,E. Salje Snippet view - 1988 |